Thermospheric density and wind retrieval from Swarm observations

• Published in: Earth, planets, and space planets, and space, 2013-01, Vol.65 (11), p.1319-1331
• Main Authors: Visser, Pieter, Doornbos, Eelco, van den IJssel, Jose, Teixeira da Encarnação, João
• Format: Article
• Language: English
• Subjects: Earth and Environmental Science; Earth Sciences; Geology; Geophysics/Geodesy
• ISSN: 1343-8832; 1880-5981
• DOI: 10.5047/eps.2013.08.003

The three-satellite ESA Swarm mission aims at mapping the Earth’s global geomagnetic field at unprecedented spatial and temporal resolution and precision. Swarm also aims at observing thermospheric density and possibly horizontal winds. Precise orbit determination (POD) and Thermospheric Density and Wind (TDW) chains form part of the Swarm Constellation and Application Facility (SCARF), which will provide the so-called Level 2 products. The POD and TDW chains generate the orbit, accelerometer calibration, and thermospheric density and wind Level 2 products. The POD and TDW chains have been tested with data from the CHAMP and GRACE missions, indicating that a 3D orbit precision of about 10 cm can be reached. In addition, POD allows to determine daily accelerometer bias and scale factor values with a precision of around 10–15 nm/s 2 and 0.01–0.02, respectively, for the flight direction. With these accelerometer calibration parameter values, derived thermospheric density is consistent at the 9–11% level (standard deviation) with values predicted by models (taking into account that model values are 20–30% higher). The retrieval of crosswinds forms part of the processing chain, but will be challenging. The Swarm observations will be used for further developing and improving density and wind retrieval algorithms.